| 印尼中苏拉威西波龙谷金矿地质特征——一种斑岩型金-银、铅、锌多金属矿床 |
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| 引用本文： | 何熙琦,刘应忠,跃连红,陈金法,陈仁.印尼中苏拉威西波龙谷金矿地质特征——一种斑岩型金-银、铅、锌多金属矿床[J].贵州地质,2011(4):272-276. |
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| 作者姓名： | 何熙琦 刘应忠 跃连红 陈金法 陈仁 |
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| 作者单位： | [1]贵州省地质调查院,贵州贵阳550005 [2]贵州省地质矿产资源开发总公司,贵州贵阳550004 |
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| 摘 要： | 波龙谷金矿床产于新生代火山岩岛弧环境。金矿体主体赋存于石英闪长玢岩岩体和岩墙之内和内、外接触带,矿石构造以细脉状、细粒浸染状为主,蚀变带和矿化带受石英闪长玢岩岩体、岩墙形态和接触带控制。矿床形成与玢岩岩体、岩墙有密不可分的关系,属于斑岩型金-银、铅、锌多金属矿床。
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| 关 键 词： | 波龙谷金矿 石英闪长玢岩 玢岩岩墙 斑岩型金-银、铅、锌多金属矿床 |
Geological Characters of Polonggu Gold Deposit in Sulawesi,Indonesia |
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| HE Xi-qi,LIU Ying-zhong,YUE Lian-hong,CHEN Jin-fa,CHEN Ren.Geological Characters of Polonggu Gold Deposit in Sulawesi,Indonesia[J].Guizhou Geology,2011(4):272-276. |
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| Authors: | HE Xi-qi LIU Ying-zhong YUE Lian-hong CHEN Jin-fa CHEN Ren |
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| Institution: | 1.Guizhou Academy of Geologic Survey,Guiyang 550005,Guizhou,China;2.Guizhou Geology and Mineral Development Co.Ltd,Guiyang 550004,Guizhou,China) |
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| Abstract: | Polonggu gold deposit occurs in volcanic island-arc environment of genozoic,the gold ore body occurs in the rock mass,dyke and the contact zone of quartz diorite porphyrite,the ore structure mainly is vein and impregnation.The alteration zone and mineralization zone are controlled by the rock mass,dyke and the contact zone of quartz diorite porphyrite.The deposit formation has deep relation with the rock mass and the dyke of porphyrite. |
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| Keywords: | Polonggu gold deposit quartz diorite porphyrite dyke of porphyrite quartz-vein gold silver lead and zinc deposit |
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